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To those who may not be aware, Lake Vostok is a subglacial fresh water lake buried under kilometres of ice, but let the following details describe it,
The Discovery of Subglacial Lake Vostok
In the 1960s, Russian scientists hypothesized water beneath the ice sheet based on results from seismic soundings. In the 1970s, a joint US-UK-Denmark airborne radar mapping project discovered areas with flat reflections from the bottom of the ice sheet suggesting water beneath the ice. The full size of Lake Vostok was first revealed in 1996 by the flat ice sheet surface mapped from the European ERS-1 satellite.
Microbial Life in Ice
Bacteria found in refrozen lake water at the bottom of the Vostok ice core could be part of an indigenous ecosystem below that's been living in the cold, dark waters for millions of years. Lake Vostok has been isolated from open exchange with the atmosphere for several million years. No one knows how any organism, cut off from air, sunlight or any apparent source of life-sustaining energy, could survive in its frigid waters or under such crushing pressure of more than 360 times the atmospheric pressure at sea level.
Subglacial Lake Vostok is the closest terrestrial analogue to Europa, the ice covered Jovian moon, and to a Neoproterozoic snowball Earth. The 4-kilometer-thick ice sheet goes afloat as it crosses the lake, just as ice sheets become floating ice shelves at the grounding line. The subglacial environment represents one of the most oligotrophic environments on Earth, an environment with low nutrient levels and low standing stocks of viable organisms. If life thrives in these environments it may have to depend on alternative energy sources and survival strategies. A flash animation illustrates the basal freezing process and the flow of the ice sheet over the lake.
The Discovery of Subglacial Lake Vostok
In the 1960s, Russian scientists hypothesized water beneath the ice sheet based on results from seismic soundings. In the 1970s, a joint US-UK-Denmark airborne radar mapping project discovered areas with flat reflections from the bottom of the ice sheet suggesting water beneath the ice. The full size of Lake Vostok was first revealed in 1996 by the flat ice sheet surface mapped from the European ERS-1 satellite.
Microbial Life in Ice
Bacteria found in refrozen lake water at the bottom of the Vostok ice core could be part of an indigenous ecosystem below that's been living in the cold, dark waters for millions of years. Lake Vostok has been isolated from open exchange with the atmosphere for several million years. No one knows how any organism, cut off from air, sunlight or any apparent source of life-sustaining energy, could survive in its frigid waters or under such crushing pressure of more than 360 times the atmospheric pressure at sea level.
Subglacial Lake Vostok is the closest terrestrial analogue to Europa, the ice covered Jovian moon, and to a Neoproterozoic snowball Earth. The 4-kilometer-thick ice sheet goes afloat as it crosses the lake, just as ice sheets become floating ice shelves at the grounding line. The subglacial environment represents one of the most oligotrophic environments on Earth, an environment with low nutrient levels and low standing stocks of viable organisms. If life thrives in these environments it may have to depend on alternative energy sources and survival strategies. A flash animation illustrates the basal freezing process and the flow of the ice sheet over the lake.